Continental crust exhibits areas of recurrent deformation and reactivation of faults that can
be persistent for hundreds of millions of years. Associated with weak lithospheric zones, the …

Previous tectonic studies have indicated that the peri-cratonic lithosphere, located away
from continental margins, is sensitive to far-field stresses propagating from active plate …

We describe new remains of notoungulates from the Cerro Azul Formation (late Miocene) in
La Pampa Province and reassign others previously studied, helping to precise the …

Climate changes related to orographic barrier uplift have been in the research spotlight over
recent years. Several works have focused on the interactions between climatic and tectonic …

In this contribution, we present the stratigraphy of the igneous and metamorphic rocks of the
Taquetrén Range, a sector located in the southernmost margin of the North Patagonian …

The syn-orogenic Miocene deposits of the Patagonian Foreland System were the focus of
numerous works in the latest years, due to their central role in the comprehension of the …

The Miocene represents a key moment in the South American evolution, since meaningful
geographic and climatic processes occurred, promoting the development of several biologic …

Abstract The Golfo San Jorge basin and other Mesozoic basins occupy extensive areas of
the extra-Andean Argentinean Patagonia. These basins initiated and evolved from the …

The interaction of tectonics and climate is considered the main determining factor in the
development of different depositional systems (from aeolian to alluvial to lacustrine …

The initial infill of the Patagonian Broken Foreland is related to Miocene, syn-orogenic,
volcaniclastic successions accommodated in intermontane basins. In the last years several …